Adaptive Predictive Inverse Control of Offshore Jacket Platform Based on Rough Neural Network     

崔洪宇  赵德有  周平 《中国海洋工程》2009,23(2):185-198

The offshore jacket platform is a complex and time-varying nonlinear system,which can be excited of harmful vibration by external loads.It is difficult to obtain an ideal control performance for passive control methods or traditional active control methods based on accurate mathematic model.In this paper,an adaptive inverse control method is proposed on the basis of novel rough neural networks (RNN) to control the harmful vibration of the offshore jacket platform,and the offshore jacket platform model is established by dynamic stiffness matrix (DSM) method.Benefited from the nonlinear processing ability of the neural networks and data interpretation ability of the rough set theory,RNN is utilized to identify the predictive inverse model of the offshore jacket platform system.Then the identified model is used as the adaptive predictive inverse controller to control the harmful vibration caused by wave and wind loads,and to deal with the delay problem caused by signal transmission in the control process.The numerical results show that the constructed novel RNN has advantages such as clear structure,fast training speed and strong error-tolerance ability,and the proposed method based on RNN can effectively control the harmfid vibration of the offshore jacket platform.  相似文献   

基于云理论、粗集和模糊神经网络的区域橡胶种植适宜度评估模型   总被引：1，自引：0，他引：1  

曹阳  宋伟东 《测绘科学》2009,34(6)

针对橡胶种植适宜性评估,基于云理论、粗集理论和模糊神经网络理论,提出了一种适宜度评估模型。该模型将转化的样本数据进行粗集简约,通过模糊神经网络得出评价因子的隶属函数,计算评价等级。研究结果表明,此模型能够科学、快速、准确地分析出橡胶种植最适宜区、适宜区、次适宜区和不适宜区。  相似文献   

Rossby waves with linear topography in barotropic fluids   总被引：1，自引：0，他引：1  

杨联贵  达朝究  宋建  张会琴  杨红丽  侯一筠 《中国海洋湖沼学报》2008,26(3):334-338

Rossby waves are the most important waves in the atmosphere and ocean, and are parts of a large-scale system in fluid. The theory and observation show that, they satisfy quasi-geostrophic and quasi-static equilibrium approximations. In this paper, solitary Rossby waves induced by linear topography in barotropic fluids with a shear flow are studied. In order to simplify the problem, the topography is taken as a linear function of latitude variable y, then employing a weakly nonlinear method and a perturbation method, a KdV （Korteweg-de Vries） equation describing evolution of the amplitude of solitary Rossby waves induced by linear topography is derived. The results show that the variation of linear topography can induce the solitary Rossby waves in barotropic fluids with a shear flow, and extend the classical geophysical theory of fluid dynamics.  相似文献   

Cascade model for fluvial geomorphology   总被引：3，自引：0，他引：3  

W. I. Newman  D. L. Turcotte 《Geophysical Journal International》1990,100(3):433-439

  相似文献   

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李永生  张景发  姜文亮  罗毅  王晓醉 《大地测量与地球动力学》2015,35(1):145-149

????????λ???????????????3????????????????????編???н??????????????????????????????????2007~2010?????20??ENVISAT ASAR?????÷????????????????????Э??????????У?????????????????й????????????Э?????????????????????3.1 mm²??????0.6mm²????????80%??e-folding???????????1.5 km?????0.21 km????????86%????????編??????Ч??У????????е??????λ?????  相似文献   

日照水库及周边区域综合地质条件分析          下载免费PDF全文

葛文海  王集宁  寻知锋  贺兆成 《山东国土资源》2015,31(1):46-49,54

日照水库是1959年建成的一座大(二)型水库,位于日照市东港区驻地以西16 km处的付疃河中游,控制流域面积548 km2,是日照城市及国民经济发展的最重要水源保障。近年来日照市经济社会飞速发展,特别随着"山东精品钢基地"等大项目的开工建设,供水安全形势愈发严峻,如何维护日照水库和保护这一水源地更是被提到了重要的议事日程。先行研究分析流域地质条件,是做好日照水库保护建设工作的重要基础。  相似文献   

对陡坡陡崖引发地质灾害的潜在影响范围进行建模分析     

章豪  温剑峰  陈温清  徐刚  史瑞洁  戴欣宜  陈杰  朱安峰  范全龙 《测绘通报》2021,(6):117-121,133

陡坡陡崖作为一种特殊的地形地貌,是造成滑坡、泥石流等各种地质灾害的重要因素之一。由陡坡陡崖引发的地质灾害会破坏人造地物,对人类的生命财产安全造成严重危害。本文利用DEM数据提取了浙江省温州市的陡坡陡崖,对温州市陡坡陡崖的影响范围进行系统研究,构建了温州市陡坡陡崖的潜在滑坡方向模型,并确定其对人造地物（如道路、房屋）的影响。本文主要研究内容有以下两个：①提取陡坡陡崖并对其潜在滑坡方向进行建模;②根据影响范围提取受影响的人造地物并建立基础数据库。结果表明,温州市的陡坡陡崖数量多,分布范围广且集中,其引发的地质灾害会对人造地物造成严重的潜在影响。本文构建的温州市基础数据库可以描述陡坡陡崖潜在影响的房屋和道路的位置,确定灾害重点防治区域,为温州市的灾害防治工作提供服务。  相似文献   

重庆“5.6”强风雹天气过程成因分析   总被引：8，自引：4，他引：8  

陈贵川  谌芸  乔林  刘德  李强  张亚萍  王文芳  张焱 《气象》2011,37(7):871-879

利用常规观测、NCEP分析场及雷达、自动站等资料对重庆＂5.6＂强风雹天气的成因进行了分析,结果表明：冷锋和副热带高空急流在风雹发生地近乎重叠的配置结构促进了次级环流的形成并有利于上升运动的强烈发展;风暴天气发生前,下垫面强烈加热、低层增温增湿、中高层干冷对大气对流不稳定性增强的作用显著;对流有效位能（CAPE）、K指数、SI指数高值区边缘的强指数梯度区、对流抑制（CIN）的小值区以及较强的垂直风切变对大风冰雹的预报有重要的指示意义;雷达回波显示多单体风暴具有三体散射、弱回波区等冰雹回波特征,中层径向辐合和反射率因子核心的反复上升下降也是形成地面大风和冰雹的重要特征;四川盆地东部东北西南向山脉对冷空气的移动有阻挡作用,山脉之间的槽状地形为多单体风暴的持续发展保留了较大的空间,明月山南麓的地形起到了强迫抬升和触发的作用,由于地形的阻挡形成狭管效应,加强了下击暴流形成的地面大风,是形成11级大风的重要因素。  相似文献   

Simulation of the Askervein flow. Part 2: Large-eddy simulations     

A. Silva Lopes  J. M. L. M. Palma  F. A. Castro 《Boundary-Layer Meteorology》2007,125(1):85-108

Large-eddy simulations of the neutrally stratified flow over the Askervein Hill were performed, to improve the knowledge of the flow obtained from field measurements and numerical simulations with Reynolds averaged Navier-Stokes (RANS) methods. A Lagrangian dynamic subgrid model was used but, to avoid the underdissipative character near the ground, it was merged with a damped Smagorinsky model. Simulations of a flat boundary-layer flow with this subgrid model showed that the turbulent vertical motions and shear stress were better resolved using grids with a stream to spanwise aspect ratio Δx / Δy = 2 than with an aspect ratio Δx / Δy = 1. Regarding the flow over the Askervein Hill, it was found that large-eddy simulations provide an acceptable solution for the mean-velocity field and better predictions of the turbulent kinetic energy in the upstream side of the hill than the model. However, as with the model, grid convergence was not achieved in the lee side and the size of the zone with reversed flow increased with the grid refinement. Nevertheless, the existence of the intermittent separation predicted with unsteady RANS in part one of this work seems unquestionable, due to the deceleration of the flow. In our opinion, a better modelling of the decelerating boundary layer in the lee side is required to improve the results obtained using equilibrium assumptions and achieve grid convergence.  相似文献   

中国海洋国土的确定及矿产资源     

王振荣  兰江华  王菲菲 《矿物岩石》2010,30(3)

我国是有辽阔海洋国土的海洋大国,海陆总国土面积约1 260×104km2。中国海处于大陆边缘,其海底地貌可分为大陆架、大陆坡、岛弧、海沟和深海海盆五大类。本文按地体构造分析我国海域及邻区的构造,其主体处于欧亚板块的华北亚板块、扬子亚板块、华南亚板块、南海亚板块和东南亚亚板块,其中亚板块可分为若干地体。台湾海岸山脉及其以东区域位于菲律宾海板块。三叠纪以来,这些板块、亚板块和地体处于不断拼合、增生或离散之中。按照联合国海洋法公约,渤海是内海。黄海的西部海域,东海和南海的大部分海域都是我国国家管辖的专属经济区,都是中国海洋国土,根本不是什么公海。我国海洋矿产资源极其丰富,海洋油气资源的勘探与开发居最重要的地位。除了已开采海滨砂矿、铜、煤等固体矿产之外,应特别要重视海洋多金属结核、天然气水合物等资源的勘探和开发。  相似文献